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mtDNA · 母亲 lineage

ND1B2

mtDNA Haplogroup ND1B2

一个家族分支的参考简介 。 共享haplogroups 无法建立家庭关系或文化认同 。

参考简介

部门背景

mtDNA 谱系分支 ND1B2 的历史背景

Origins and Evolution

mtDNA haplogroup ND1B2 is a subclade of ND1B within the broader ND1 lineage. Based on the phylogenetic position beneath ND1B (itself rooted in East–Northeast Asia) and the pattern of downstream variation, ND1B2 most likely diversified during the Late Pleistocene to early Holocene (post-Last Glacial Maximum) as populations occupying northeastern Eurasia underwent localized differentiation and postglacial expansion. The lineage reflects maternal continuity in parts of Siberia, the Amur region, northern Japan, and adjacent coastal zones where ND1B and related D/ND1 lineages are common.

Because the observed dataset for ND1B2 is limited (reported in a small number of modern samples and two ancient individuals), its internal phylogeny is shallow compared with older pan-Eurasian mtDNA haplogroups; this pattern is consistent with a regional founder effect, episodes of genetic drift in hunter-gatherer groups, and localized demographic events during the Holocene.

Subclades (if applicable)

At present, ND1B2 appears to have few well-differentiated downstream subclades in published datasets. Available sequence diversity suggests short branch lengths, indicating a relatively recent split from ND1B and limited subsequent diversification, although additional sampling (especially full mitogenomes from Siberia, the Amur region, northern Japan and coastal forager populations) could reveal finer substructure. The paucity of deeply divergent subclades points to demographic processes such as founder effects, small effective population sizes, and localized continuity rather than broad continent-wide expansion.

Geographical Distribution

ND1B2 shows a concentrated northeast Asian distribution with detectable presence in several population contexts:

  • Northeast Asia and Siberia: Most detections are in Siberian and Tungusic/Mongolic-affiliated groups and other communities of the Amur–Okhotsk region, reflecting long-term regional continuity.
  • Northern Japan and Jomon-descended groups: ND1B2 or closely related ND1B variants are occasionally found among Ainu and other populations with partial Jomon ancestry, consistent with coastal forager connections.
  • Mainland East Asia: Low to moderate, localized occurrences among Han Chinese, Japanese and Koreans likely reflect later admixture and gene flow from northeastern sources.
  • Central and Southeast Asia: Sporadic low-frequency occurrences are best interpreted as the product of historic east–west and coastal dispersals or drift.

The haplogroup has been identified in two archaeological samples in available databases, tying it to Holocene contexts in northeastern Eurasia and supporting its role in late Pleistocene–Holocene regional population structure.

Historical and Cultural Significance

ND1B2 is primarily informative for reconstructing regional maternal continuity rather than representing a broad demographic event. It helps clarify links among:

  • Paleolithic and early Holocene Siberian populations, whose maternal lineages contributed to later northern Eurasian genetic structure;
  • Jomon-related and northern Japanese groups, where ND1B and related lineages mark continuity of coastal-forager ancestries;
  • Subarctic and coastal forager communities, where founder effects and drift often elevated certain mtDNA variants.

Because the lineage is relatively rare in large-scale modern datasets, ND1B2 is most valuable in archaeogenetic and regional population studies that aim to trace maternal line continuity, postglacial recolonization routes, and local demographic events rather than continent-spanning migrations.

Conclusion

mtDNA ND1B2 is a regionally focused maternal lineage of northeastern Eurasia that arose after the diversification of ND1B. Its limited diversity and low-to-moderate frequency distribution point to localized demographic histories — founder effects, drift, and continuity among coastal and inland foraging communities — and make it a useful marker for studies of Late Pleistocene to Holocene population dynamics in Siberia, the Amur region, and northern Japan. Expanded mitogenome sampling in understudied northeast Asian groups and additional ancient DNA finds will be essential to refine its internal branching and timing.

关键点

  • Origins and Evolution
  • Subclades (if applicable)
  • Geographical Distribution
  • Historical and Cultural Significance
  • Conclusion
参考简介

树形关系( N)

phylgenetic 上下文和子拼写

进化路径

沿已记录的上级分支追溯至 ND1B2。年代为估计值,可能随参考数据更新而调整。

步骤 单倍群 年龄估计 考古时代 时间流逝 直系后裔 被测试的现代后裔 古代连接
1 ND1B2 当前 ~16,000 years ago Mesolithic 16,000 years 0 0 0
2 ND1B ~28,000 years ago Paleolithic 28,000 years 2 0 0
3 ND1 ~42,000 years ago Paleolithic 42,000 years 2 0 0
4 ND ~45,000 years ago Paleolithic 45,000 years 1 0 12
5 N ~60,000 years ago Paleolithic 60,000 years 16 26,150 13
6 L3 ~70,000 years ago Paleolithic 70,000 years 7 30,162 6
7 L3'4 - - - 2 30,212 0
8 L3'4'6 - - - 2 30,216 0
9 L2'3'4'6 - - - 2 31,333 0
10 L2'3'4'5'6'7 - - - 2 31,349 0
11 L1'2'3'4'5'6'7 - - - 2 31,852 0
12 L ~160,000 years ago Paleolithic 160,000 years 2 32,236 5

Subclades (0)

终端分支 -没有记录的子密钥

Siblings (1)

来自同一父分支的分支( oplogroup)

参考简介

哪里是这个世界

地理分布和现代存在

记录来源

East / Northeast Asia

现代发行

The populations where mtDNA haplogroup ND1B2 is found include:

  1. East Asian populations (Han Chinese, Japanese, Koreans)
  2. Northeast Asian and Siberian groups (Yakut, Evenks, various Tungusic and Mongolic peoples)
  3. Ainu and Jomon-descended populations of northern Japan
  4. Indigenous peoples of Arctic and subarctic regions (where related D/ND1 lineages occur)
  5. Tibetan and Himalayan populations (low to moderate, localized occurrences)
  6. Central Asian minorities (low frequencies reflecting east–west contact)
  7. Coastal East Asian forager/seafaring groups (enrichment of specific downstream variants)
  8. Ancient Paleolithic and early Holocene remains from Siberia and northeastern Eurasia (archaeogenetic contexts)
  9. Small, localized occurrences in parts of Southeast Asia (downstream dispersals or genetic drift)
  10. Sporadic / low-frequency detections in broader East Eurasian datasets (reflecting historic gene flow and sampling variance)
历史背景

分枝穿越时间

大致历史时间范围内的估计形成情况:周期标志提供了背景,并不意味着与特定文化的联系。

  1. ~20k 年前

    上一个冰川最大值

    上一个冰河时代的高峰,人口隔离

  2. ~16k 年前

    Haplogroup ND1B2

    此 mtDNA 分支的形成时间为推定值,日期和地点仅作参考。

    这个分支
  3. ~10k 年前

    新石器革命

    农业开始,定居社区形成

  4. ~5k 年前

    青铜时代

    金属加工、书写和早期文明

  5. ~3k 年前

    铁器时代

    铁工具,扩大贸易网络

  6. ~2.5k 年前

    古典时代

    希腊和罗马文明蓬勃发展

  7. 现

    现日

    现代时代

参考简介

考古学背景

已记录的 mtDNA 分支 ND1B2 考古关联

有记录的协会

这些标签描述与 ND1B2 相关的参考样本所处的考古背景。仅凭这种关联,无法判断所有携带者都属于某种文化或沿同一路线迁徙。

Altai Neanderthal Bohemian Hunter-Gatherer Chagyrskaya Les Cottes Mezmaiskaya Paleolithic Cultures Peștera cu Oase
文化任务基于古代DNA样本的考古背景,可能代表特定时期的区域协会.
MATERNAL LINEAGE · ANCIENT DNA

古代世系证据地图

跟随母舰飞向这个分支 探索古代载体的发现地点

正在装入古老的观测...

标记是考古发现地点。一个破碎的连接器是连续分支之间一种不确定的、拟议中的地理过渡,辅以多个日期的观察;它不是一个准确的旅行路线、出生地或直接血统的证明。父系样本可能属于其他后代分支。在证据不足的地方,差距依然存在。样本日期与随机群形成日期不同。

数据

数据证明( P)

来源信息和数据质量

上次更新 2026-02-16
信心分数 50/100
覆盖范围 Low

数据来源

分类、估计日期和地理背景反映了所记录的参考数据,随着证据的修订而可能发生变化,样本覆盖范围不均匀;所记录的地点和考古协会没有确定个人出身或文化特征。